2 inches per year.
The Mid Atlantic Ridge
The Mid-Atlantic Ridge is an example of a divergent plate boundary, where tectonic plates move away from each other. It is characterized by seafloor spreading, where magma rises from the mantle to create new crust. This process contributes to the widening of the Atlantic Ocean.
The Mid-Atlantic Ridge has one of the slowest rates of seafloor spreading, averaging about 2.5 cm per year. This ridge is located in the Atlantic Ocean and is less active compared to other spreading ridges like the East Pacific Rise.
destructive plate boundary
Countries that are part of the mid-ocean ridge spreading centers include Iceland, located on the Mid-Atlantic Ridge, and parts of Antarctica, where the East Pacific Rise intersects the Southern Ocean. These areas are often remote and not associated with specific countries.
Iceland is spreading apart from the Mid-Atlantic ridge. Iceland is a hot spot on the ridge
Sea floor spreading
The Mid-Atlantic Ridge is a divergent plate boundary, also known as a spreading center.
The Mid-Atlantic Ridge is a spreading center located in the middle of the Atlantic Ocean.
no
The Mid-Atlantic Ridge is actually spreading slower than the East Pacific Rise. The rate of seafloor spreading along the Mid-Atlantic Ridge is estimated at about 2.5 centimeters per year, while the East Pacific Rise spreads at a rate of about 5 centimeters per year.
The Mid Atlantic Ridge
+- 2 cm per year
No, it is actually one of the slowest spreading ridge on Earth. The slowest ridge is the Southwest Indian ridge, while the East Pacific Rise is the fastest.
One example would be...the mid-atlantic ridge.
he discover sea floor spreading
One example would be...the mid-atlantic ridge.